Abstract

Information on environmental conditions shaping archaeal communities thriving at the seafloor of the central Pacific Ocean is limited. The present study was conducted to investigate the diversity, composition, and function of both entire and potentially active archaeal communities within Pacific deep-sea sediments. For this purpose, sediment samples were taken along the 180° meridian of the central Pacific Ocean. Community composition and diversity were assessed by Illumina tag sequencing targeting archaeal 16S rRNA genes and transcripts. Archaeal communities were dominated by Candidatus Nitrosopumilus (Thaumarchaeota) and other members of the Nitrosopumilaceae (Thaumarchaeota), but higher relative abundances of the Marine Group II (Euryarchaeota) were observed in the active compared to the entire archaeal community. The composition of the entire and the active archaeal communities was strongly linked to primary production (chlorophyll content), explaining more than 40% of the variance. Furthermore, we found a strong correlation of the entire archaeal community composition to latitude and silicic acid content, while the active community was significantly correlated with primary production and ferric oxide content. We predicted functional profiles from 16S rRNA data to assess archaeal community functions. Latitude was significantly correlated with functional profiles of the entire community, whereas those of the active community were significantly correlated with nitrate and chlorophyll content. The results of the present study provide first insights into benthic archaeal communities in the Pacific Ocean and environmental conditions shaping their diversity, distribution, and function. Additionally, they might serve as a template for further studies investigating archaea colonizing deep-sea sediments.

Highlights

  • Archaea play a key role in global biogeochemical cycles [1,2,3,4]

  • The lowest ferric oxide and manganese dioxide concentrations were measured at stations 10 and 12, respectively, whereas the highest concentrations were determined at station 2

  • The total organic carbon (TOC) content as a general indicator for nutrient availability fluctuated around 0.6% of the sediment dry weight

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Summary

Introduction

Archaea play a key role in global biogeochemical cycles [1,2,3,4]. These microorganisms are widely distributed in various environments such as permafrost [5], hot springs [6, 7], hypersaline lakes [8], marine seawaters [9], and freshwater as well as marine (deep-sea) sediments [10,11,12]. Deep-sea sediments constitute one of the largest ecosystems on earth, covering approximately 65% of its surface. This ecosystem is characterized by extreme conditions including high pressure, cold temperatures, and lack of light. These communities are generally dominated by archaeal taxa belonging to the phyla Thaumarchaeota and Euryarchaeota [11, 13, 16,17,18]

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